Ozone thesis

The developed countries account for 1. Consequently, sea levels are rising and major flooding has started to occur in cities and agricultural areas. Schneider 21, Both substances are stable and react similar to CFCs in the stratosphere to deplete the ozone.

Being a natural constituent of the stratosphere, O3 is regularly formed and destroyed in a cyclic manner with solar radiation as the driving force. Scientists have noticed a significant decrease in fish and seabird populations.

Plants are dying from the UV exposure. Thus, there are no natural processes that remove the ODS from the lower atmosphere. The Heat is On.

Free essays on Environment posted on this site were donated by anonymous users and are provided for informational use only. The recipe for making ozone starts off with oxygen molecules. Higher levels of UV radiation cause plankton to be less productive. There is no connection between particulate aerosols and pressurized products also called aerosols.

The O3 readily absorbs UV light and dissociates into its constituent components. For the ozone layer to return to its natural state, the chlorine loading which is presently 3 ppbv has to be brought down to a level below 2 ppbv. This makes the food chain vulnerable as plankton is the lowest food source on the chain.

The ozone layer serves a vital purpose in the stratosphere as it blocks out harmful ultraviolet rays. However, that same stability allows these same CFCs to repetitively deplete our ozone for the next years. In scientists discovered a hole in the stratospheric ozone layer over Antarctica.

In the absence of any other disturbances, O3 settles into a dynamic steady state in which the rate of its formation is equal to the rate of its destruction.

Carbon dioxide has the ability to absorb high amounts of infrared energy, thus producing heat, and thereby warming the atmosphere. In nature O3 is formed in the stratosphere when ultraviolet light strikes an oxygen molecule.

The earth which sustains us is in need of loving care.

Not all chlorine and bromine sources contribute to ozone layer depletion. In the stratosphere, new ozone molecules are constantly created in chemical reactions fueled by power from the sun.

Similarly, the invention of the automobile made travel easier and quicker.

This process helps to maintain a steady temperature on the earth. It is used as a disinfectant and bleaching agent. When Less is not Enough. Unless we heed her call and immediately tend to her wounds, she will be unable to sustain us as she has in the past. Research has shown that ozone depletion occurs over the latitudes that include North America, Europe, Asia, and much of Africa, Australia, and South America.

Our glaciers are melting, our seas are rising, and our coasts are eroding away. For example, researchers have found that chlorine from swimming pools, industrial plants, sea salt, and volcanoes does not reach the stratosphere.Depletion of ozone and formation of ozone hole • Ozone, in fact is a gas having fishy smell and O3 molecules which works as the protective shield for the life in the earth.

It absorbs solar ultraviolet radiations and thereby protects life on the earth from several damage such as DNA mutation, skin cancer, blood cancer, etc. Owens is a community college that focuses on your success; in fact, it's our mission.

We have resources to get you on the career path you've always wanted and provide you with convenient class times and caring faculty. ii OZONE AND LUNG FIBROSIS Ashwini Katre MS in Public Health in the Department of Environmental Health and Toxicology ABSTRACT Ozone is an extremely reactive gas molecule composed of three oxygen atoms.

Environment term papers (paper ) on The Destruction of the Ozone Layer: INTRODUCTION In the beginning man lived simply and harmoniously with earth. However, as time progressed mankind's thirst for. ozone layer keeps getting bigger and bigger.

Each year since the late s, much of the protec- BEYOND DISCOVERY BEYOND DISCOVERY This article was published in and has not been updated or revised.